Sessional papers of the Dominion of Canada 1905 . uncovering them. The section published with the map of the Costigan coal basin isintended to show the relation of each of these areas to one another orthe construction of the ranges. It extends from the Sawback rangeeastward to the first or outer range of the Rocky mountains, and in-cludes three basins of Cretaceous rocks. To the west of the Sawbacka fault has brought up against the highest of the Paheozoic, rockscomparable to the series in the Castle mountain, probably of Cambrianage. Eastward, then to the edge of the Cretaceous, there is a co
Sessional papers of the Dominion of Canada 1905 . uncovering them. The section published with the map of the Costigan coal basin isintended to show the relation of each of these areas to one another orthe construction of the ranges. It extends from the Sawback rangeeastward to the first or outer range of the Rocky mountains, and in-cludes three basins of Cretaceous rocks. To the west of the Sawbacka fault has brought up against the highest of the Paheozoic, rockscomparable to the series in the Castle mountain, probably of Cambrianage. Eastward, then to the edge of the Cretaceous, there is a contin-uous series down to below the Intermediate series which is Devonian. (^jnlbajcll!^^^lraoftfi^la!la. ^^
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